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Appendix A. EasyFlux DL CR6CP Process Flow
A-5
Calculate covariances of
H
2
O
and wind components for each lagged
dataset and do coordinate rotation on covariances.
⇩
Find the dataset with the physically possible lag that maximizes the
covariance of
H
2
O
and vertical wind. Use this dataset for the
FLUX_AMERIFLUXFORMAT and FLUX_CSFORMAT output tables. If
any results are invalid, continue with lag of zero. (See
EasyFlux DL
CR6OP
manual, Appendix D on Frequency Corrections.)
⇩
Calculate the frequency correction factor for covariances of
H
2
O
and
rotated wind components, taking into account attenuation from block
averaging, line averaging, spatial separation, and tube attenuation.
(See
EasyFlux DL CR6OP
manual, Appendix D on Frequency
Corrections, Ibrom et al 2007, Brugon et al. 2016, and program code.)
⇩
Calculate final momentum flux from rotated and frequency corrected
covariances of u with w and v with w.
⇩
Apply SND correction to the rotated and frequency corrected
covariance of w and Ts.
⇩
Calculate specific heat of ambient (moist) air and calculate final
sensible heat flux.
⇩
Calculate scaling temperature (used for data quality grading). (See
EasyFlux DL CR6OP
manual Appendix F on Data Quality Grading.)
⇩
Calculate Bowen Ratio
⇩
Calculate the overall quality grades for fluxes of sensible heat, latent
heat, and
CO
2
. (See
EasyFlux DL CR6OP
manual, Appendix F on
Data Quality Grading.)
⇩
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